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Improving models of the Earth’s magnetic field for directional drilling applications

机译:为定向钻井应用改进地球磁场模型

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摘要

Over the past 20 years, directional borehole drilling has become increasingly important for improving the optimal extrac­tion of reserves from challenging targets and for reducing wellbore collisions. Very long wells drilled using borehole steering methods can take weeks to months to complete and rely on accurate models of the Earth’s magnetic field which necessarily include a parameterization of its time variation. Magnetic field models used in the hydrocarbon industry, such as the BGS Global Geomagnetic Model (BGGM), are computed from data collected by a network of ground-based magnetic observato­ries and from low Earth-orbiting satellites. Magnetic field models provide napshots looking back in time, but to be useful to industry, they also need to predict how the field will change in the future. Previously, predictions of magnetic variation have been based on relatively simple extrapolation of the observed changes. We introduce a physics-based technique to forecast the changes in the field by deducing large-scale flow of the iron-rich liquid at the top of the outer core and use this to advect the present magnetic field forwards in time. We demonstrate that this method produces valuable improvements in the accuracy of magnetic field models and hence an improved tool for directional drilling.
机译:在过去的20年中,定向井眼钻探对于提高从具有挑战性的目标中最佳地提取储量和减少井眼碰撞变得越来越重要。使用井眼转向方法钻的超长油井可能需要数周至数月才能完成,并依赖于地球磁场的精确模型,该模型必然包括其时间变化的参数化。碳氢化合物行业中使用的磁场模型,例如BGS全球地磁模型(BGGM),是根据地面磁观测网络和低地球轨道卫星收集的数据计算得出的。磁场模型提供了回溯时的小憩,但要对行业有用,他们还需要预测未来磁场的变化。以前,磁变化的预测是基于观察到的变化的相对简单的推断。我们引入一种基于物理学的技术,通过推断外铁芯顶部的富铁液体的大规模流动来预测磁场的变化,并利用它及时对当前磁场进行平移。我们证明了这种方法在磁场模型的准确性方面产生了有价值的改进,因此是一种用于定向钻探的改进工具。

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